期刊文献+

内部磁场梯度引起的扩散对NMR岩石测量响应的影响 被引量:5

Effects of diffusion due to internal gradients on NMR response in rocks
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摘要 低场NMR岩心分析能够刻度NMR测井响应,对于较为准确地预测储层的渗透率、束缚水体积等与产能密切相关的参数尤其重要.对来自南海东部油田的100%饱和盐水的砂岩岩心进行了变回波间隔的实验室NMRT2测量,随着回波间隔的增大对实验观测到的两种不同的T2分布的移动进行了理论上的分析和解释.随着回波间隔的增加,T2谱向着长弛豫时间的移动可以用过优化NMR采集参数消除掉,而对另外一种由内部磁场梯度引起的移动即随着回波间隔增加T2谱向短弛豫时间的移动则复杂得多,至今为止也无法做到定量化内部磁场梯度的值,这种移动能够引起错误的NMR测井解释.因此理解内部磁场梯度对T2弛豫时间的影响是很有必要的.文中对由内部磁场梯度扩散引起的扩散弛豫对T2弛豫时间的影响进行了理论上的模拟计算,这有助于理解和解释岩石内部磁场梯度对NMRT2弛豫时间的影响.最后结合压汞毛管压力曲线,解释了具体的岩心实验结果,并且计算了具体的岩心的内部磁场梯度值,计算出的内部磁场梯度值应该被视为内部磁场梯度的几何平均值. Calibration of the NMR log response using low field lab NMR measurements of core samples is important for the accurate prediction of permeability and bulk volume of irreducible water related strongly to reservoir productivity. NMR CPMG T2 measurements were performed on the sandstone cores from east oilfield, South China Sea, at multiple echo spacings at 100% brine saturated state. Two different shifts in the T2 distributions with increasing echo spacing are found and the theoretical analysis and interpretation is given about the two different shifts. The shift of the T2 peaks towards longer relaxation times can be eliminated by choosing short enough echo spacing. But the other shift of the T2 peaks towards shorter relaxation times due to complicated internal field gradient can cause errors in the interpretation of the T2 distributions and up to now there is no good way to quantify internal field gradients. Thus it is important to understand the effects of diffusion on T2 relaxation times due to internal field gradients. The theoretical simulation results of the effects of diffusion-induced dephasing on the T2 distribution due to magnetic field gradients are calculated, which is helpful to understand and explain the impacts of internal magnetic field gradients on NMR T2 relaxation time. Finally, combined with mercury injection curves, the core measurement results are explained and the internal magnetic field gradients of two cores are calculated, which should be regarded as geometric mean of internal field gradients distribution.
出处 《地球物理学进展》 CSCD 北大核心 2007年第2期556-561,共6页 Progress in Geophysics
基金 中海石油(中国)有限公司深圳分公司重点研究项目(Z2005SLSZ-082)资助
关键词 内部磁场梯度的影响 两种不同的T2移动 实验室NMR测量 回波间隔 effects of internal magnetic field gradients, two different shifts of T2 distribution, Lab NMR measurements, echo spacings
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  • 1刘堂晏,肖立志,傅容珊,王忠东.球管孔隙模型的核磁共振(NMR)弛豫特征及应用[J].地球物理学报,2004,47(4):663-671. 被引量:50
  • 2何雨丹,毛志强,肖立志,任小军.核磁共振T_2分布评价岩石孔径分布的改进方法[J].地球物理学报,2005,48(2):373-378. 被引量:208
  • 3谢然红,肖立志,邓克俊,廖广志,刘天定.二维核磁共振测井[J].测井技术,2005,29(5):430-434. 被引量:48
  • 4王筱文,肖立志,谢然红,张元中.中国陆相地层核磁共振孔隙度研究[J].中国科学(G辑),2006,36(4):366-374. 被引量:20
  • 5施良骐 刘树山.2GPa固体围压三轴试验装置的设计研究.第一届高温高压岩石力学学术讨论会论文集[M].北京:学术期刊出版社,1988.122-129. 被引量:1
  • 6[1]Schirov M, Legchenko A. A new direct non-invasive groundwater detection technology for Australia. Exploration Geophysics, 1991,22(2): 333 ~ 338 被引量:1
  • 7[2]Goldman M, Rabinovich B, Rabinovich M,et al. Application of the integrated NMR-TDEM method in groundwater exploration in Israel.Journal of Applied Geophysics, 1994, 31(4): 27 ~ 52 被引量:1
  • 8[3]Yaramanci U, Lange G, Knodel K. Surface NMR within a geophysical study of an aquifer at Haldensleben( Germany). Geophysical Prospecting, 2000,47(5): 923 ~ 943 被引量:1
  • 9[7]Trushkin D V, Shushakov O A, Legchenko A V. Surface NMR applied to an electro-conductive medium. Geophysical Prospecting,1995, 43(4): 623 ~ 633 被引量:1
  • 10[8]Shushakov O A, Legchenko A V. Groundwater proton magnetic resonance in the horizontally stratified media of different electrical conductivity. Geology and Geophysics(In Russian), 1994, 35(10): 140~ 145 被引量:1

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